People get confused as to what is an earthquake, and an aftershock and they may be used interchangeably.
Earthquake and aftershock are relative terms. Generally, the aftershocks represent minor adjustments at the time of the earthquake or a foreshock. The earthquakes and the aftershocks depend on the magnitude of each. Historically, deep earthquakes are less likely to be followed by an aftershock than shallow earthquakes.
Earthquake vs Aftershock
The main difference between earthquake and aftershock is that earthquake is known as mainshock. They are more powerful and long-lasting. The magnitude of an earthquake is stronger, whereas aftershocks come after the earthquakes and are less powerful than earthquakes, the magnitude of an aftershock is lower.
Earthquakes are high magnitude natural calamities that bring great devastation. They happen when friction occurs, which then causes the slow movement of the tectonic plates. Places that are located near the tectonic plates are known to have more quakes than places that are far off.
The small tremors that are felt after the mainshock is called an aftershock. An aftershock is considered a smaller earthquake. They are of lower magnitude than earthquakes. An earthquake is a sign that an aftershock will happen.
Comparison Table Between Earthquake and Aftershock
| Parameters of Comparison | Earthquake | Aftershock |
| What is it | An earthquake is a slow movement of the earth’s crust. | An aftershock is a small tremor that is felt after the mainshock or the earthquake. |
| Causes of occurrence | An earthquake happens because of the slow movement of the earth’s crust. They can happen due to man-made activities like mining, nuclear blasts, etc. | Aftershocks happen when the earth’s crust fixes itself after the tremor. |
| Duration | The earthquake can last about 4 minutes. | The lasting of the aftershocks depends on the magnitude of the earthquake, generally, they last for a few hours, but they can last for up to months. |
| Magnitude | The earthquake has a higher magnitude than an aftershock. | An aftershock has a lower magnitude than an earthquake. |
| Certainty | Earthquake is difficult to predict. It can happen anywhere. | Aftershocks come after the mainshocks, so it is easy to predict. |
| Destruction caused | Earthquake of higher magnitude causes high destruction. | As aftershocks have a lower magnitude so there is no damage or very little damage. |
What is Earthquake?
An earthquake is a movement of the earth’s crust. An earthquake happens when friction happens in the earth’s crust leading to a crack in the crust. The slow and steady movement of the tectonic plates causes earthquakes. Places that are located near the tectonic plates are known to have more earthquakes than places located far from the tectonic plates.
In earthquakes, the pressure that is released radiates out, and these waves cause the ground to shake. Sometimes, due to the vibrations, the man-made objects are damaged depending on the magnitude of the quake and cause volcanic eruptions or tsunami.
An earthquake is the main shock that can be felt. They may come in different strengths. The higher the strength, the more damage will happen. The magnitude of an earthquake is measured through the Richter magnitude scale. The earthquakes last up to a few minutes.
An earthquake is a sudden tremor and comes without any warning. They can be a result of some of mankind’s activities like mining, nuclear testing, etc. The earthquakes cannot be predicted.
What is Aftershock?
An aftershock is a smaller magnitude earthquake. The more frequent the earthquake is, the more frequent the aftershocks are. Aftershocks can even happen on a regular basis after the earthquakes.
They are mainly of lower magnitude than earthquakes. If the aftershock has a higher magnitude than the previous shock, then it is referred to as the mainshock, and the previous shock is called a foreshock.
They cause no damage or less damage than earthquakes. People expect aftershocks after the quack with a higher magnitude.
They happen in the first few minutes of the mainshock, depending on the earthquake. The magnitude of the aftershocks also depends on the magnitude of the earthquake or the mainshock.
Generally, aftershocks are of the same nature as earthquakes or mainshocks, but they are not as strong as the quakes and do not cause much damage.
The frequency of the aftershocks decreases with time.
Main Differences Between Earthquake and Aftershock
- The magnitude of the earthquake is much stronger than the aftershock.
- An earthquake of higher destruction causes higher destruction, whereas aftershocks are usually of low magnitude they cause little or no damage.
- An earthquake happens due to the movement of the tectonic plates, whereas the aftershocks happen as the earth’s crust adjust itself.
- An earthquake is followed by the aftershocks within a few hours of the mainshock.
- If the aftershock is stronger than the earthquake, then that the aftershock is renamed as the mainshock, and the earthquake is reamed as foreshocks.
- An earthquake cannot be predicted by anyone, whereas an aftershock can be predicted as they always come after the mainshock or the earthquake.
- An earthquake happens around the places located near the tectonic plates, whereas the aftershocks happen after the earthquake.
Conclusion
Earthquakes, aftershocks, and foreshocks are relative terms.
A quake of the highest magnitude is called an earthquake. The quakes that are come before the mainshock are called foreshocks. The quakes that are followed after the mainshocks are called aftershocks.
An earthquake is the movement of the tectonic plates in the earth’s crust. The magnitude of the earthquake is higher than the foreshocks and the aftershocks.
Foreshocks are quakes that precede before the higher magnitude earthquakes. The magnitude of foreshocks depends.
Aftershocks are the smaller quakes that are followed after the mainshock. The magnitude of aftershocks also depends.
They all are relative terms, but they have a key difference between them.
References
- https://www.jstage.jst.go.jp/article/jpe1952/4/2/4_2_63/_article/-char/ja/
- https://ascelibrary.org/doi/abs/10.1061/(ASCE)ST.1943-541X.0001019